The Pliocene-Pleistocene boundary in pelagic oozes off Reunion Island, western Indian Ocean

• Autorzy: Duczmal-Czerniewicz A. , Jugowiec-Nazarkiewicz M. , Szydło A.
• Języki publikacji: EN

Abstrakty

EN

Nannoplankton and foraminifera from the pelagic oozes from a water depth of 3 684 meters, 150 km southeast of Reunion Island, Indian Ocean, prove the NN18 and NN19 nannoplankton zones, indicating the Pliocene.Pleistocene boundary. The Pliocene.Pleistocene boundary was established at 220.230 cm depth. The abundance of Globorotalia truncatulinoides increases from about 50 cm below the sea floor. The microfossil assemblages and clay mineral components of the sediments may be correlated with changes of climatic conditions influenced by glaciations.

Słowa kluczowe

EN

biostratigraphy; calcareous nannoplankton; foraminifers; Indian Ocean; pelagic ooze; Reunion Island

PL

biostratygrafia; muł pelagiczny; nanoplankton wapienny; Ocean Indyjski; Reunion

• Wydawca: Faculty of Geology of the University of Warsaw ; Komitet Nauk Geologicznych PAN
• Czasopismo: Acta Geologica Polonica
• Rocznik: 2006
• Tom: Vol. 56, no. 4
• Strony: 407--419
• Opis fizyczny: Bibliogr. 39 poz.,Il., rys.,

Twórcy

autor

Duczmal-Czerniewicz A.

autor

Jugowiec-Nazarkiewicz M.

autor

Szydło A.

• Institute of Geology, Adam Mickiewicz University, Maków Polnych Str. 16, PL 61-686 Poznań, Poland,

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